A Damage Constitutive Model for a Rock under Compression after Freeze-Thaw Cycles Based on the Micromechanics

The freeze-thaw cycles will cause continuous damage to the rock, which is much related to the microcrack length, rock permeability, and frost heaving pressure. However, the failure mechanism of the rock under compression after freeze-thaw cycles is not very clear; therefore, it is studied with the d...

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Main Authors: Hongyan Liu, Xiaochen Zhang, Xidong Yan
Format: Article
Language:English
Published: Hindawi-Wiley 2021-01-01
Series:Geofluids
Online Access:http://dx.doi.org/10.1155/2021/3177464
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spelling doaj-a2d860244443421ea47f533fa753da572021-08-02T00:00:57ZengHindawi-WileyGeofluids1468-81232021-01-01202110.1155/2021/3177464A Damage Constitutive Model for a Rock under Compression after Freeze-Thaw Cycles Based on the MicromechanicsHongyan Liu0Xiaochen Zhang1Xidong Yan2College of Engineering & TechnologySchool of Safety EngineeringRIOH Transport Consultants LtdThe freeze-thaw cycles will cause continuous damage to the rock, which is much related to the microcrack length, rock permeability, and frost heaving pressure. However, the failure mechanism of the rock under compression after freeze-thaw cycles is not very clear; therefore, it is studied with the damage theory here. First of all, according to the hydraulic pressure theory, the relationship between the frost heaving pressure and the microcrack propagation length in one single microcrack is established based on the elastoplastic mechanics and fracture theory. Second, by assuming the total strain of the rock under compression is comprised of the initial damage strain, elastic strain, additional damage strain, and plastic damage strain, a constitutive model for a rock based on the deformation and propagation of the microcrack under compression after freeze-thaw cycles is established. Finally, the proposed model is verified with the test result. In all, the proposed model can perfectly reflect the deterioration of the rock mechanical behavior under compression after the freeze-thaw cycles.http://dx.doi.org/10.1155/2021/3177464
collection DOAJ
language English
format Article
sources DOAJ
author Hongyan Liu
Xiaochen Zhang
Xidong Yan
spellingShingle Hongyan Liu
Xiaochen Zhang
Xidong Yan
A Damage Constitutive Model for a Rock under Compression after Freeze-Thaw Cycles Based on the Micromechanics
Geofluids
author_facet Hongyan Liu
Xiaochen Zhang
Xidong Yan
author_sort Hongyan Liu
title A Damage Constitutive Model for a Rock under Compression after Freeze-Thaw Cycles Based on the Micromechanics
title_short A Damage Constitutive Model for a Rock under Compression after Freeze-Thaw Cycles Based on the Micromechanics
title_full A Damage Constitutive Model for a Rock under Compression after Freeze-Thaw Cycles Based on the Micromechanics
title_fullStr A Damage Constitutive Model for a Rock under Compression after Freeze-Thaw Cycles Based on the Micromechanics
title_full_unstemmed A Damage Constitutive Model for a Rock under Compression after Freeze-Thaw Cycles Based on the Micromechanics
title_sort damage constitutive model for a rock under compression after freeze-thaw cycles based on the micromechanics
publisher Hindawi-Wiley
series Geofluids
issn 1468-8123
publishDate 2021-01-01
description The freeze-thaw cycles will cause continuous damage to the rock, which is much related to the microcrack length, rock permeability, and frost heaving pressure. However, the failure mechanism of the rock under compression after freeze-thaw cycles is not very clear; therefore, it is studied with the damage theory here. First of all, according to the hydraulic pressure theory, the relationship between the frost heaving pressure and the microcrack propagation length in one single microcrack is established based on the elastoplastic mechanics and fracture theory. Second, by assuming the total strain of the rock under compression is comprised of the initial damage strain, elastic strain, additional damage strain, and plastic damage strain, a constitutive model for a rock based on the deformation and propagation of the microcrack under compression after freeze-thaw cycles is established. Finally, the proposed model is verified with the test result. In all, the proposed model can perfectly reflect the deterioration of the rock mechanical behavior under compression after the freeze-thaw cycles.
url http://dx.doi.org/10.1155/2021/3177464
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AT xiaochenzhang adamageconstitutivemodelforarockundercompressionafterfreezethawcyclesbasedonthemicromechanics
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